托福閱讀TPO28(試題+答案+譯文)第1篇:Groundwater
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托福閱讀原文
【1】Most of the world’s potable water—freshwater suitable for drinking is accounted for by groundwater, which is stored in the pores and fractures in rocks. There is more than 50 times as much freshwater stored underground than in all the freshwater rivers and lakes at the surface. Nearly 50 percent of all groundwater is stored in the upper 1,000 meters of Earth. At greater depths within Earth, the pressure of the overlying rock causes pores and cracks to close, reducing the space that pore water can occupy, and almost complete closure occurs at a depth of about 10 kilometers. The greatest water storage, therefore, lies near the surface.
Aquifers, Porosity and Permeability
【2】Groundwater is stored in a variety of rock types. A groundwater reservoir from which water can be extracted is called an aquifer. We can effectively think of an aquifer as a deposit of water. Extraction of water depends on two properties of the aquifer: porosity and permeability. Between sediment grains are spaces that can be filled with water. This pore space is known as porosity and is expressed as a percentage of the total rock volume. Porosity is important for water—storage capacity, but for water to flow through rocks, the pore spaces must be connected. The ability of water, or other fluids, to flow through the interconnected pore spaces in rocks is termed permeability. In the intergranular spaces of rocks, however, fluid must flow around and between grains in a tortuous path; this winding path causes a resistance to flow. The rate at which the flowing water overcomes this resistance is related to the permeability of rock.
【3】Sediment sorting and compaction influence permeability and porosity. The more poorly sorted or the more tightly compacted a sediment is, the lower its porosity and permeability. Sedimentary rocks—the most common rock type near the surface—are also the most common reservoirs for water because they contain the most space that can be filled with water. Sandstones generally make good aquifers, while finer-grained mudstones are typically impermeable. Impermeable rocks are referred to as aquicludes. Igneous and metamorphic rocks are more compact, commonly crystalline, and rarely contain spaces between grains. However, even igneous and metamorphic rocks may act as groundwater reservoirs if extensive fracturing occurs in such rocks and if the fracture system is interconnected.
The Water Table
【4】The water table is the underground boundary below which all the cracks and pores are filled with water. In some cases, the water table reaches Earth’s surface, where it is expressed as rivers, lakes and marshes. Typically, though, the water table may be tens or hundreds of meters below the surface. The water table is not flat but usually follows the contours of the topography. Above the water table is the vadose zone, through which rainwater percolates. Water in the vadose zone drains down to the water table, leaving behind a thin coating of water on mineral grains. The vadose zone supplies plant roots near the surface with water.
【5】Because the surface of the water table is not flat but instead rises and falls with topography, groundwater is affected by gravity in the same fashion as surface water. Groundwater flows downhill to topographic lows. If the water table intersects the land surface, groundwater will flow out onto the surface at springs, weather to be collected there or to subsequently flow farther along a drainage. Groundwater commonly collects in stream drainages but may remain entirely beneath the surface of dry stream-beds in arid regions. In particularly wet years, short stretches of an otherwise dry stream-bed may have flowing water because the water table rises to intersect the land surface.
[Glossary]
Sediment: materials (such as sand or small rocks) that are deposited by water, wind, or glacial ice.
Topography: the shape of a surface such as Earth’s, including the rise and fall of such features as mountains and valleys.
托福閱讀試題
1.In paragraph 1, why does the author mention "the pressure of the overlying rock"?
A.To show how water can be forced deep under Earth's surface.
B.To show why groundwater is more plentiful than surface freshwater.
C.To correct a commonly made error about the location of groundwater.
D.To explain why most groundwater lies near Earth's surface.
2.According to paragraph 1, groundwater differs from the water in riversand lakes in terms of its
A.portability.
B.usefulness.
C.abundance.
D.cost.
3.The word "extracted" in the passage(paragraph 2)is closest in meaning to
A.used.
B.poured.
C.removed.
D.kept out.
4.The word "termed" in the passage(paragraph 2)is closest in meaning to
A.considered.
B.called.
C.limited to.
D.caused by.
5.According to paragraph 2, what does porosity determine?
A.The rate at which the aquifer's water overcomes resistance to flow.
B.The amount of water that the aquifer can hold.
C.The likelihood that fractures and joints will occur in the aquifer.
D.The depth underground at which the aquifer lies.
6.According to paragraph 2, what is the relationship between permeability and porosity?
A.The more pores a rock has, the higher its porosity but the lower its permeability.
B.Rocks with many internal spaces that are not connected with each other will have high porosity but low permeability.
C.If water flows through a rock easily, it has high permeability but low porosity.
D.Rocks that have high permeability have high porosity and vice versa.
7.The word "compacted" in the passage(paragraphy 3)is closest in meaning to
A.hard.
B.compressed.
C.heavy.
D.deeply buried.
8.According to paragraph 3, when can igneous rock serve as an aquifer?
A.When it has many connected fractures.
B.When it lies next to metamorphic rock.
C.When it lies relatively near the surface.
D.When it is crystalline.
9.The word "coating" in the passage(paragraph 4)is closest in meaning to
A.stream.
B.barrier.
C.amount.
D.layer.
10.Paragraph 4 implies which of the following about the rootsof plants?
A.They prevent water from reaching the vadose zone.
B.They mark the boundary between the vadose zone and the water table
C.They do not typically get their water from the water table.
D.They help keep the water table from dropping farther.
11.Which of the sentences below best expresses the essential information in the highlighted sentence in the passage paragraph 5 ? Incorrect choices change the meaning in important ways or leave out essential information.
A.Groundwater only flows out of the ground if the water table intersects the land surface.
B.If the land surface and the water table intersect, groundwater can flow underground.
C.Groundwater may be drained if springs occur where the water table intersects the land surface.
D.Where the water table meets the land surface, groundwater flows out through surface springs.
12.Paragraph 5 implies which of the following about the level of the water
A.It may rise or fall from year to year, depending on annual rainfall.
B.It does not vary in arid regions.
C.It rarely intersects the land surface of most regions.
D.It is unrelated to the rate at which groundwater flows.
13. Look at the four squares [■] that indicate where the following sentence could be added to the passage.Where would the sentence best fit? This is a consequence of the slow rate of movement of the groundwater, which often prevents the water table from attaining a flat (horizontal) level.
The water table is the underground boundary below which all the cracksand pores are filled with water. In some cases, the water table reaches Earth's surface, where it is expressed as rivers, lakes and marshes. ■【A】Typically,though,the water table may be tens or hundreds of meters below the surface. ■【B】The water table is not flat but usually follows the contours of the topography. ■【C】Above the water table is the vadose zone, through which rainwater percolates. ■【D】Water in the vadosezone drains down to the water table, leaving behind a thin coating of water onmineral grains. The vadose zone supplies plant roots near the surface withwater.
14. Directions: An introductory sentence for a brief summary of the passage is provided below. Complete the summary by selecting the THREE answer choices that express the most important ideas in the passage. Some sentences do not belong in the summary because they express ideas that are not presented in the passage or are minor ideas in the passage. This question is worth 2 points.
Most of the world's potable water is stored as groundwater in the poresand fractures of underground rock, much of it at depths of less than 1,000 meters.
A.Sedimentary rock may make poor aquifers because of tightly compacted sediment, which reduces porosity and permeability.
B.Porosity is a measure of the empty space within rock while permeability measures the degree to which water can flow freely through rock.
C.In arid regions, the water tables remain at a constant level far below the surface, preventing stream-beds from filling up even during wet years.
D.Groundwater reservoirs are characterized by the porosity and permeability of the rock in which they lie, and these factors vary according to the type of rock.
E.The vadose zone is typically dry because water does not stay in it, but instead percolates down to aquifers below or drains out through springs and streams.
F.Although the water table usually follows the contours of the land surface, its level may vary from year to year and may intersect to the surface in places.
托福閱讀答案
1.在高亮部分的描寫(xiě)之后，本段的最后一句出現(xiàn)了，therefore。這里也是在說(shuō)the pressure of the overlying rock導(dǎo)致的結(jié)果，也就是文章提到它的目的。其結(jié)果是，大部分的水儲(chǔ)都在比較表面的地方。所以其目的就是要解釋為什么水都在表面的地方。
2.對(duì)應(yīng)原文第二句話(huà)，也就是將地下水和江河湖泊水進(jìn)行比較的那句話(huà)。原句說(shuō)more than 50 times。就證明是地下水的水量大。這里A是飲用性，原文并沒(méi)有說(shuō)江水不能喝。B是有用，同理。D是代價(jià)。這個(gè)就更沒(méi)提到了。所以答案為C豐富。
3.extract本身是汲取，取出的意思。從原文后面一句話(huà)可以推測(cè)，因?yàn)楹竺嬲f(shuō)儲(chǔ)水土層可以看作是對(duì)一筆水存款，所以前面應(yīng)該是說(shuō)可以取出。另外這個(gè)詞的詞綴ex-本身就有出的意思。那么A是使用，B是潑出，C是移動(dòng)，D是隔離在外。
4.term作名詞是術(shù)語(yǔ)，這個(gè)很常用。而這里用了其動(dòng)詞否定形式，那么應(yīng)該是…被術(shù)語(yǔ)為，也就是被命名為。那么A是認(rèn)為，B是叫做，C是限制于，D是由于。所以應(yīng)該選B。
5.A決定于permeability of rack，對(duì)應(yīng)本段最后一句。B正確，對(duì)應(yīng)本段第七句(porosity is important for water-storage capacity)，這句話(huà)只要根據(jù)porosity定位就很好找。C和porosity沒(méi)有直接關(guān)系。D原文就沒(méi)提到。
6.對(duì)應(yīng)本段第一句和第二句，即sorting和compaction會(huì)共同影響permeability，結(jié)合上一段的最后一句理解，多孔性分為兩種情況，一種是孔多但是互相不聯(lián)通，這時(shí)permeability不高;另一種是孔多并且互相聯(lián)通，那么porosity高的同時(shí)permeability也會(huì)高。因此選擇B。其他幾個(gè)選項(xiàng)的敘述都不完整。這兩者的關(guān)系并不是簡(jiǎn)單的正比例。
7.compact是壓縮，緊密的意思。通過(guò)后面的and的并列內(nèi)容可以推出其詞義，因?yàn)閍nd后面說(shuō)rarely contain space，那就是說(shuō)中間的空間很小。所以選擇B壓縮的。A是堅(jiān)硬，C是重的，D是深埋的。
8.對(duì)應(yīng)本段文章最后一句"even igneous rocks may act as groundwater…"后半句給出的就是答案，那么它說(shuō)的是要有fractures并且要interconnected。所以選A。
9.Coating本來(lái)是外衣，和涂層的意思。那么A是溪流，B是障礙物，C是數(shù)量，D是層。所以D符合。
10.根據(jù)plant roots定位到本段最后一句。說(shuō)vadose zone給植物根部提供了水。選項(xiàng)A，B，D都沒(méi)提到。而只有C沒(méi)有錯(cuò)誤，因?yàn)閜lant roots是從vadose zone汲取的水份，而不是water table。所以選C。
11.A選項(xiàng)缺少了spring這個(gè)條件;B，C選項(xiàng)不正確。D包含了原文所有的主干部分，正確。
12.根據(jù)這段最后兩句對(duì)于wet year的描寫(xiě)可以得出根據(jù)降雨量不同，地下水位是有變化的。所以A正確。B不正確，原文明顯寫(xiě)到在arid regions降雨量多時(shí)干燥的溪床會(huì)有水。C也不對(duì)，整段都有大篇幅在寫(xiě)和land surface的intersects。D原文沒(méi)提到。
13.要插入的句子說(shuō)this is a consequence，那么this一定指代什么，根據(jù)后半句可以知道指代的內(nèi)容應(yīng)該與地下水位不是平面有關(guān)。所以C的位置符合，因?yàn)榍懊嬉痪湔f(shuō)地下水位不是平面。
14.A 錯(cuò)誤，對(duì)應(yīng)文章第三段的第三句有關(guān)于sedimentary rock的描寫(xiě)。根據(jù)原文，sedimentary rock是很好的aquifers，B正確，對(duì)應(yīng)第二段的前四句。C正確，對(duì)應(yīng)原文第二段。D錯(cuò)誤，vadose zone中會(huì)留下thin coating所以還是會(huì)濕潤(rùn)。對(duì)應(yīng)原文第四段。E錯(cuò)誤，water table本非remain at a constant level，根據(jù)倒數(shù)第二句，地下水位有時(shí)會(huì)和地表交叉的。F正確，對(duì)應(yīng)原文最后一段。
托福閱讀譯文
【1】世界上絕大部分飲用水----可以飲用的淡水----都是地下水，它們儲(chǔ)藏在巖石孔隙和裂縫中。儲(chǔ)藏于地下的淡水是地表淡水河流和湖泊中總水量的50倍。大約50%的地下水存在于地下深1000m以?xún)?nèi)的地層中。隨深度增加，上覆巖層壓力使巖石孔隙和裂縫閉合，減少了水的儲(chǔ)存空間，而超過(guò)10公里深的地下孔隙幾乎全部閉合。因此絕大部分水儲(chǔ)存于接近地表的地層中。
水層，孔隙度和滲透率
【2】地層水儲(chǔ)存在多種巖石中。可以取出的地下水的聚集層叫做水層。我們可以認(rèn)為水層即水的聚集地層。從地層中取水取決于水層的兩個(gè)因素：孔隙度和滲透率。沉積顆粒之間的空間可以?xún)?chǔ)存水，這種孔隙空間由孔隙度表征?？紫抖仁菐r石孔隙體積與總體積的百分比?？紫抖葘?duì)地層儲(chǔ)水能力尤為重要，但欲使水從巖石中流出，孔隙之間必須相互連通。水或其它流體從相互連通的孔隙中流動(dòng)的能力即為滲透率。在粒間孔發(fā)育的巖石中，流體必須在顆粒周?chē)那弁ǖ乐辛鲃?dòng);這種曲折通道會(huì)對(duì)流動(dòng)產(chǎn)生阻力。水克服阻力流動(dòng)的速率與巖石滲透率相關(guān)。
【3】沉積物的分選性和壓實(shí)程度影響其滲透率和孔隙度。巖石分選越差或壓實(shí)越緊則其孔隙度和滲透率越低。沉積巖----地表最常見(jiàn)的巖石----也是最常見(jiàn)的水儲(chǔ)集層，因?yàn)樗鼈兂в凶疃嗟目梢詢(xún)?chǔ)水的孔隙空間。砂巖一般是最好的儲(chǔ)水層，但小顆粒的泥巖則通常不可滲透。不滲透巖層都稱(chēng)為隔水層?；鸪蓭r和變質(zhì)巖壓實(shí)更緊，通常有結(jié)晶，并幾乎沒(méi)有粒間孔隙。但是即便是火成巖和變質(zhì)巖也可因裂縫大量發(fā)育并相互連接而成為儲(chǔ)水層。
地下水位
【4】地下水位指地層巖石裂縫和孔隙充滿(mǎn)水的邊界。某些情況下，地下水位可能到達(dá)地表，在那里它以河流、湖泊或沼澤地的形式存在。但通常情況下地下水位位于地面數(shù)十或數(shù)百米以下。地下水位不是水平的，而是通常沿著地勢(shì)起伏。地下水位以上稱(chēng)為包氣帶，在這里降水得以過(guò)濾。包氣帶中的水會(huì)沉降到地下水位，只在礦物顆粒表面留下一層水膜。包氣帶為地表附近植物根部提供水分。
【5】因?yàn)榈叵滤槐砻娌⒎撬剑茄刂貏?shì)起伏，地下水和地表水受到重力影響的模式相同。地下水沿著下傾地層流向地勢(shì)低洼處。如果地下水位與地表相交，地下水將以噴泉的形式流出地面，要么就地聚集，要么沿排水通道流向更遠(yuǎn)的地方。地下水通常在小溪中聚集，但在干旱地區(qū)也可能全部停留在干涸河床下。在特定濕潤(rùn)的年月里，一段干涸的河床下游可能有水流動(dòng)，因?yàn)榈叵滤惶搅四抢锏牡乇硪陨稀?/p>
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托福閱讀TPO28(試題+答案+譯文)第1篇:Groundwater
